Abstract
The crystal structures of three different solid-solution members between the new mineral oxyvanite (V3O5) - and berde- sinskiite (V2TiO5) from a quartzite rock in the Pereval marble quarry of the Sludyanka complex, south of Lake Baikal (Russia), have been refined in space group C2/c (a � 10.0, b � 5.0, c � 7.0 A ˚ , b � 111 � ) from X-ray single-crystal diffraction-data. The composition of the studied crystals, determined by electron-microprobe analyses, is: ðV 3þ
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